Review articles

Soil-related terroir factors: a review


A “terroir” is a cultivated ecosystem in which the vine interacts with the soil and the climate. The soil influences vine development and grape ripening through soil temperature, water supply and mineral supply. Soil temperature has a significant effect on vine phenology. Limited water supply to the vines restricts shoot and berry growth, which is critical for reaching a suitable grape composition to produce high-quality red wines. Secondary metabolites, like polyphenols (anthocyanins, tannins) and aroma compounds or their precursors, are impacted in particular by vine water status. Among nutrients vines pick up from the soil, nitrogen plays a key role. Nitrogen influences vine vigor, yield, berry size and grape composition. Low nitrogen supply stimulates the synthesis of polyphenols, while it can negatively impact certain aroma compounds in grapes and wines. Over the past decades, tools have been developed to quantify terroir parameters. Vine water status can be assessed by means of carbon isotope discrimination measured on grape sugar (so-called δ13C). Vine nitrogen status can be assessed with the measurement of Yeast Available Nitrogen (YAN). In this way, terroir parameters can not only be measured but also mapped. Ideally, vineyards should be established in areas where soil temperature (relative to air temperature), soil water holding capacity (relative to rainfall and potential evapotranspiration) and soil nitrogen availability are optimum for the type of wine which is intended to be produced. Terroir expression can, however, be optimized by choosing appropriate plant material, and via vineyard floor management, fertilization and other management techniques.

Terroir expression in winegrowing and the specific role of the soil

In wine production, quality and style are considered to be impacted by the place where the vines grow. This relation between the sensory attributes of a wine and its origin is referred to as “terroir”, a French word which cannot easily be translated into English. The official definition according to the International Organization of Vine and Wine (OIV, 2010) is that « Vitivinicultural “terroir” is a concept which refers to an area in which collective knowledge of the interactions between the identifiable physical and biological environment and applied vitivinicultural practices develops, providing distinctive characteristics for the products originating from this area. “Terroir” includes specific soil, topography, climate, landscape characteristics and biodiversity features ». A more condensed definition is provided by Seguin (1988), who considers terroir « as an interactive ecosystem, in a given place, including climate, soil and the vine ». Human factors should also be considered when referring to “terroir”, because terroir expression implies, at a minimum, a history of winegrowing in a given place and also the intervention of men to optimize terroir expression (van Leeuwen and Seguin, 2006). Many factors are involved in terroir expression. Among these, climate, soil, and cultivar obviously are of major importance. All of these factors interact, which makes it impossible to consider the optimum for each factor when taken separately (van Leeuwen, 2010). It is, for instance, not possible to refer to the ideal climate for producing high-quality wines, without taking into account the local soil type and cultivar. Because so many factors are involved, it makes sense to propose a hierarchy of their influence on vine phenology, vine development, and grape composition. In a trial where 37 variables were measured on nine parcels with three soils, and three grapevine varieties over five consecutive vintages (climate effect), van Leeuwen et al. (2004) investigated for each variable the percentage of the total variance attributable respectively to the climate, soil and temperature effect. Vine development and phenology were predominantly driven by the climate, except total shoot length and ripening speed (Figure 1a). Yield parameters were equally impacted by the soil and the climate, with cluster number being more impacted by the climate and cluster weight by the soil (Figure 1b). Berry composition was mainly driven by the climate, in particular all components linked to acidity. Berry nitrogen and total anthocyanins were mostly influenced by the soil type. Berry sugar was equally impacted by the soil and the cultivar (Figure 1c). Vine mineral status was predominantly determined by the soil type (Figure 1d) while all parameters linked to vine water status were equally impacted by the soil and the climate (Figure 1e). Note that all parcels were dry-farmed. In sum, soil and climate determine water and nitrogen supply to the vines which, in turn, controls vegetative and reproductive development.

Figure 1. Percentage of variance attributable to climate, soil, and cultivar effect for a) vine development and phenology, b) yield components, c) grape composition, d) vine mineral status and e) vine water status (computed from van Leeuwen et al., 2004). All parcels located in Saint-Emilion (Bordeaux area), vintages spanning the period 1996-2000.

Soil and terroir expression

Vineyard soils are diverse and soil type impacts wine quality

Great wines are produced on a wide diversity of soils, including gravelly soil on Quaternary alluvium (in Pauillac, Bordeaux, Table 1a), clayey lime-rich soil on Jurassic limestone (in Mazis-Chambertin, Burgundy, Table 1b) and heavy clay soil on Paleogene substratum (in Saint-Emilion, Bordeaux, Table 1c).

Table 1. Soil composition in three famous vineyards located on a) gravelly soil developed on Quaternary alluvium in Pauillac, Bordeaux, b) clayey lime-rich soil developed on Jurassic limestone in Mazis-Chambertin, Burgundy and c) heavy clay soil on Paleogene substratum in Saint-Emilion, Bordeaux.

It is surprising how diverse these soils are, although they are all located in highly prestigious estates. High-quality potential vineyard soils may be coarse (Table 1a) or fine textured (Table 1b and 1c), have high (Table 1b) or low pH (Table 1a), and may be rich (Table 1a) or poor in organic matter content (Table 1c). It is obvious from these examples that no straight forward relationship can be established between soil composition and wine quality. Vineyard soils are also often modified by human intervention. The high copper content, in particular in the soil from the Bordeaux area (Table 1c), is the result of copper sprayings to protect the vines against downy mildew.

There is, however, proof that soil type influences wine quality, as shown by Trégoat (2003) and Renouf et al. (2010). These authors mapped the soils of seven of the most prestigious estates of the Bordeaux area at high resolution (between 1/1000th and 1/5000th), covering 400 ha of vineyards. Soils were classified according to the French “Référentiel pédologique” classification (Baize and Girard, 1995). Predominant soil type was identified for each parcel. These estates produce generally three wines, according to three levels of quality. Grapes are fermented separately by the parcel of origin and only the best lots of wine are blended into the 1st quality wine, which is the only one being marketed with the full name of the estate. A quality index was constructed, based on the frequency with which the wine from a given parcel integrated the 1st quality and a rating was accordingly attributed to each parcel and averaged over a five year period. Nine major soil types were identified (Figure 2), with PEYROSOL (gravelly soil on Quaternary alluvium) being the predominant soil type. Highest quality was produced on PLANOSOL (soil with heavy clay subsoil of Tertiary origin), ARENOSOL (sandy soil of Quaternary aeolian origin), BRUNISOL (sandy-gravel soil on Quaternary alluvial terraces) and PEYROSOL (gravelly soil on Quaternary alluvial terraces) (Figure 3). Quality was lowest on COLLUVIOSOL (deep sandy soil on colluvium from Quaternary substratum), LUVISOL (leached sandy clay soil on Quaternary alluvium) and REDUCTISOL (sandy soil with permanent water table, located in talwegs on Quaternary substratum). This study shows that wine quality varies significantly according to soil type, although it does not explain which mechanisms are involved.

Figure 2. Frequency of soil types identified in seven highly prestigious Bordeaux estates.

Figure 3. Quality potential index, based on the frequency with which the wine produced on a given soil type is blended into the highest quality wine, for the nine major soil types identified in seven highly prestigious Bordeaux winegrowing estates.

Different approaches to study vineyard soils

Experts from different scientific backgrounds study vineyard soils, resulting in a diversity of approaches. Geologists study the parent material (Wilson, 1998) and geomorphologists the topography (Fanet, 2001). Soil scientists map vineyard soils (van Leeuwen et al., 1989) and agronomists study soil physical and chemical composition (Seguin, 1986). Soil microbiologists analyze the microbial community of vineyard soils (Bokulich et al., 2014; Gilbert et al., 2014). All these approaches provide useful information, but generally remain highly descriptive. Another drawback is that most scientists stick to the tools they are familiar with and in a sense “are prisoners of their own discipline” (Moran, 2001). Yet, there are many factors involved in terroir expression, which implies that terroir studies have to be multi-disciplinary. If the soil has an impact on grape composition and wine quality, it is necessarily mediated through the vine. In order to explain the effect of terroir on wine composition, interactions between the soil and the vine (and possibly the climate) need to be taken into account. This paper deals with the soil effect in terroir expression, through its impact on vine physiology. The soil provides anchorage to the vine, minerals, water and a specific temperature regime in the root zone. Hence, the understanding of its effect on terroir needs to be focused on the effect of soil temperature, soil water supply, and soil mineral supply on vine development, phenology and grape ripening dynamics. Moreover, contrary to geological outcrops or soil types, these variables can be quantified.

Major soil-related parameters in terroir expression that can potentially be quantified: temperature in the root zone, soil mineral supply, and soil water supply

Soil temperature in the root zone

The timing of ripeness is critical in the production of wines offering specific characteristics in relation to their origin. If grapes ripen too early in the season in warm conditions, those grapes are high in sugar and low in organic acids. Wines produced from such grapes are unbalanced and lack freshness. Moreover, aromatic complexity is reduced in warm ripening conditions (Pons et al., 2017). If grapes ripen too late in the season, they may not reach full ripeness, with the resulting wines tending to be acidic and showing an excess of green flavors. The ideal window for reaching ripeness is roughly situated between the 10th of September and the 15th of October in the Northern Hemisphere, or March in the Southern Hemisphere (van Leeuwen and Seguin, 2006). The timing of phenology (budburst, flowering and veraison) is mainly driven by air temperature (Parker et al., 2011) and the specific temperature requirements of the grapevine variety (Parker et al., 2013). To remain within the ideal ripening window, growers who are looking for optimal terroir expression adapt their choice of the grapevine variety to local climatic conditions so as to plant early ripening varieties in cool climates and late ripening varieties in warm climates (van Leeuwen and Seguin, 2006). Soil temperature in the root zone also impacts phenology, but does so in a less decisive way compared to air temperature. Soil temperature depends on energy balance, which is related to soil color and albedo (proportion of sunlight reflected on the soil), slope steepness and direction. It is also highly impacted by water content, because water has a high specific caloric capacity: wet soils warm up more slowly compared to dry soils (Tesic et al., 2002). Soil temperature is also related to soil structure. According to Steenwerth and Belina (2008), soil management (cover crop versus tillage) does not have a major impact on soil temperature.

In vineyards where the combination of local climatic conditions and the precocity of the major grapevine variety results in ripening late in the ideal calendar window, a warm soil in the root zone (either because of low water content or shallow rooting) generally results in better wines. This is clearly the case with Cabernet franc in the Loire Valley (Bodin and Morlat, 2006), Cabernet-Sauvignon in the Bordeaux area (van Leeuwen, 2001) and Cabernet-Sauvignon in Hawke’s Bay, New Zealand (Tesic et al., 2002). For these varieties in these locations, soil temperature is critical to produce high-quality wines. For varieties ripening in the middle of the ideal ripening window (e.g. Merlot in Bordeaux or Cabernet-Sauvignon in Napa, California), soil temperature has little impact on quality performance. Cool soils may be an advantage in warm climates because they can slightly delay ripeness, although this aspect is poorly documented.

Soil mineral supply (except nitrogen)

Soil supplies vines with minerals, including major elements (N, P, K, Mg, Ca) and trace elements (Fe, Bo, Mn, Zn, among others). Except for nitrogen, which will be addressed in the next section, there is little evidence that soil minerals are major drivers of terroir expression. In popular wine books, terroir expression is repeatedly attributed to « deep roots picking up trace elements » but no demonstration is provided on how these elements could possibly be transformed into aroma compounds or other sensory attributes of wines (Moran, 2001; Maltman, 2013). Seguin (1986) found no close relation between soil minerals and wine quality, and this was confirmed by van Leeuwen et al. (2004). This does not mean that soil minerals have no impact whatsoever. Excess in available soil potassium can possibly increase pH in must and wines (Morris et al., 1983; Soyer and Molot, 1993). High potassium levels are found in soils derived from specific rocks containing large amounts of feldspar, illite and mica (volcanic rocks, slate or shale; Huggett, 2006) or can be the result of excessive fertilization (Dundon et al., 1984). Many famous winegrowing sites are developed on parent material containing limestone, inducing the presence of high available soil calcium (Champagne, Burgundy, Saint-Emilion, Loire Valley in France, Tuscany in Italy, la Rioja in Spain and Coonawarra in Australia) (Wilson, 1998; Fanet, 2001). However, high soil calcium is not a prerequisite for good vineyard soil, because some of the world’s most renowned wines are produced on acidic soils developed on Quaternary alluvium, with low calcium content (Table 1a; Seguin, 1986). The depicted positive effect of calcium may be indirect. High calcium improves soil structure (White, 2003), which in turn improves root penetration, speeds up soil warming in the spring and improves internal drainage. The presence of active lime also reduces soil organic matter turnover, limiting the availability of mineral nitrogen (Duchaufour, 2001).

Soil nitrogen supply

Nitrogen is a highly important nutrient in all agricultural crops, including grapevines. The level of nitrogen supply influences vine vigor, crop level, berry size, and impacts both major metabolites of the grape (sugar, organic acids) and secondary metabolites (phenolic compounds, aromas and aroma precursors) (Keller, 2010). The soil availability of nitrogen to the vine is not easy to estimate, because the vast majority of nitrogen in the soil is in organic form, which is not directly accessible to the vines. The organic matter first has to be turned into mineral nitrogen by soil microorganisms (including Nitrosomonas and Nitrobacter) before it can be absorbed by the vines, predominantly as NO3-. This is a complex and dynamic process, which depends on many factors: soil aeration, soil temperature, soil humidity, soil pH, and the type of organic matter, in particular its C/N ratio (van Leeuwen et al., 2000). The amount of available mineral nitrogen is clearly linked to the soil type and, thus, makes it part of the “terroir” effect (van Leeuwen, 2010), although it can obviously also be manipulated through fertilization practices (Spayd et al., 1993, 1994) and vineyard cover crop management.

In the production of red table wines, moderate nitrogen supply is an important quality-enhancing factor. Vine vigor is related to nitrogen supply (Figure 4). Low nitrogen supply limits berry size and berry malic acid content, and it increases sugar content and phenolic content (Tregoat et al., 2002). 3-Isobutyl-2-methoxypyrazine (IBMP), a major green flavor in grapes and wines, considered detrimental in red wines, is not directly impacted by vine nitrogen status (Helwi et al., 2015). However, high vigor induced by high nitrogen supply potentially increases bunch shading, which may increase berry IBMP content. In white wine production, the desired level of nitrogen supply is higher in comparison with red wine production. In Sauvignon blanc, nitrogen increases the synthesis of volatile thiol precursors (volatile thiols are major aroma compounds in many grapevine varieties, including Sauvignon blanc, generally considered being positively associated with wine quality). Because nitrogen also stimulates the synthesis of glutathione (a compound that preserves aroma compounds in musts and wines) and limits the production of tannins (that are involved in volatile thiol degradation), moderately high nitrogen supply to the vines is desired in white wine production, at least for those varieties dependent on volatile thiols for their aromatic signature (Choné et al., 2006; Helwi et al., 2016). Excessive nitrogen supply is not desired either, because it increases susceptibility of grapes to grey rot (Botrytis cinerea; Mundy, 2008). It is important to note that optimum nitrogen supply is different in red and white wine production. This observation explains, at least partially, why some soils are better for the production of high-quality white wines and others for the production of high-quality red wines.


Figure 4. Relations between vine nitrogen status and vigor in a Bordeaux vineyard (Château Fombrauge, Saint-Emilion) in 2016: a) Vine nitrogen status, assessed by the measurement of Yeast Available Nitrogen (YAN) at harvest; b) Vine vigor, assessed by the measurement of winter pruning weight; and c) correlation between YAN and pruning weight. Maps were obtained by Inverse Distance Weighting (IDW) interpolation from results from 10 samples/ha.

Some authors have attributed a major role to soil microorganisms in terroir expression, although they remain relatively vague about the mechanisms involved in this potentially beneficial effect (Bourguignon, 1995). It is true that a healthy soil should have at least some minimum level of microbiological activity, because soil microorganisms play a major role in the transformation of organic nitrogen into mineral nitrogen. Without this process, vines would not survive because of severe nitrogen deficiency. Microbial interactions in vineyard soils are, however, highly complex, and our current state of knowledge provides no evidence that higher microbiological activity induces higher quality and enhances terroir expression. Very high microbiological activity in the soil would simply result in excessive nitrogen release, which is often detrimental to wine quality, in particular in red wine production (Choné et al., 2001). Soil microbiology has recently received increased attention because it has been shown that the soil microbiome is terroir-specific (Bokulich et al., 2014; Gilbert et al., 2014). However, the study by Bokulich et al. (2014) does not clearly show a functional impact of diverse microbiological communities across geographical origins on grape composition, or wine sensory attributes. The study of vine health and longevity supported by healthy biomes are additional areas of research which need further investigation.

Soil water supply

Vine water status depends on climatic parameters (rainfall and reference evapotranspiration), the capacity of the soil to store water, the transpiration rate of the vines, rooting depth, and, when applied, irrigation practices. The impact of soil and climate on vine water status is similar in magnitude (van Leeuwen et al., 2004; Figure 1e). Depletion of soil water reserves can be simulated with a water balance model (Lebon et al., 2003). Soil water is stored in soil porosity. Except for water-logged soils, water is drained out of the large soil pores (>10 μm in diameter). Water located in extremely small pores (<0.2 μm in diameter) cannot be extracted by vine roots. Pores within the 0.2 μm to 10 μm range can store water against deep drainage and progressively release it to the vines. The percentage of total soil volume within this range of pore size varies with soil texture: approximately 5% in a very sandy soil, 10% in a very clayey soil, and 20% in a very silty soil (Saxton et al., 1986). Hence, soil texture has a major impact on soil water holding capacity (SWHC). It is also extremely dependent on rooting depth and percentage of coarse elements. SWHC of vineyards is highly variable, covering a range from 50 mm in very shallow soils with a sandy texture and having a high percentage of coarse elements, to over 350 mm in silty soils, which allow deep rooting (van Leeuwen et al., 2009). When a water table is present within the reach of the roots (in the case of water-logged soils), SWHC can be considered infinite, because water consumed by the vines will be replaced through lateral soil-water movements.

Vine water status has a major impact on vegetative and reproductive growth, fruit composition and wine quality. Evidence that regular, but limited, water supply to the vines is a major factor explaining the terroir effect was first published in the 1960s (Seguin, 1969) and confirmed many times since (Duteau, 1987; van Leeuwen and Seguin, 1994; Trégoat et al., 2002; van Leeuwen et al., 2004; Storchi et al., 2005; Bodin and Morlat, 2006; Koundouras et al., 2006; de Andrès-de-Prado et al., 2007; van Leeuwen et al., 2009; Tramontini et al., 2013; Picard et al., 2017). Limited water supply leads to shoot growth cessation (Table 2; van Leeuwen and Seguin, 1994; Pellegrino et al., 2005) and restrains berry growth, in particular when water deficits occur pre-veraison (Table 2; Ojeda et al., 2001; van Leeuwen et al., 2004). Water deficit also reduces berry malic acid content (Table 2; van Leeuwen and Seguin, 1994). The impact of water deficit on berry sugar content is non-linear: grape sugar is increased under mild water deficit because of reduced carbon allocation to shoots, but grape sugar is reduced under severe water deficit because of restrained photosynthesis (van Leeuwen et al., 2009). Water deficit increases skin phenolics, in particular anthocyanins (Table 2; Duteau et al., 1981; Ojeda et al., 2002; Trégoat et al., 2002; Ollé et al., 2011), which is a major asset in the production of high-quality red wines. Limited water supply to the vines increases glycoconjugates of major aromas in red grapes (Koundouras et al., 2006) and improves the aging bouquet of fine red wines (Picard et al., 2017) and their global quality (Table 2; Koundouras et al., 2006). Severe water deficit stress, however, can impair red wine quality. Vine water deficit is not necessarily a major driver of white wine quality, because their aromas may be negatively impacted (Peyrot des Gachons et al., 2005; Pons et al., 2017). Strong water deficit negatively impacts aromas from the volatile thiol family and thus depreciates the quality of white wines produced from Sauvignon blanc and, probably, of all varieties which depend on volatile thiols for their aromatic typicity (Peyrot des Gachons et al., 2005).

Table 2. Correlation coefficients between vine water status (as assessed by water potential measurements), and veraison (day of the year), shoot growth, yield parameters, and grape composition. Compiled from van Leeuwen and Seguin, 1994; Trégoat et al., 2002; van Leeuwen et al., 2004; Koundouras et al., 2006; and van Leeuwen et al., 2009. Note that water potentials are negative and become more negative with increasing water deficit; hence, positive correlations indicate a decrease with water deficit and negative correlations an increase.


Saint-Emilion (Bordeaux)

Saint-Emilion (Bordeaux area)

Nemea (Greece)


Saint-Emilion (Bordeaux)


Cabernet franc

Merlot, Cabernet franc and Cabernet-Sauvignon






1996, 1997, 1998 1999, 2000

1997, 1998


2004, 2005, 2006, 2007

Number of observations







van Leeuwen and Seguin, 1994

van Leeuwen et al., 2004

Koundouras et al., 2006

Trégoat et al., 2002

van Leeuwen et al., 2009

Indicator of water deficit

average pre-dawn leaf water potential veraison - harvest

minimum pre-dawn leaf water potential veraison - harvest

average pre-dawn leaf water potential veraison - harvest

pre-dawn leaf water potential at ripeness

minimum stem water potential over the season

Shoot growth cessation (Day of the Year)






Total shoot length (cm)






Veraison (Day of the Year)






Berry weight (g)






Yield (kg/vine)






Grape sugar (g/L)






Total acidity (g tartrate/L)












Malic acid (g/L)






Tartaric acid (g/L)






Sugar/Acid ratio






Grape anthocyanins (mg/L)






Wine anthocyanins (mg/L)






Total phenolics (index)






Ripening speed






Global wine quality (rating)












Significance: *, **, *** represents significance at p< 0,05, 0,01 and 0,001 respectively; NS: non significant


Terroir expression and irrigation

One of the major driving factors behind terroir expression is the occurrence of moderate water deficits, in particular for red wines. Hence, full irrigation is not compatible with terroir expression. In very dry areas, excessive water stress can impair yields and possibly grape quality potential. In the Mediterranean basin, growers have developed over the past millenniums training systems and selected plant material which allows grape production in extremely dry conditions. In New World production areas, irrigation is frequently implemented to obtain economically sustainable yields and avoid major damage to vines and grapes under dry conditions. It is striking though that some of the most famous wines in the New World are grown in dry-farmed vineyards (Hill of Grace in Australia, Dominus Estate in Napa, California, Montebello Ridge in the Santa Cruz Mountains, California). When necessary, irrigation should be maintained at a minimum, to allow water deficits to develop over the season. It is not easy to mimic moderate water deficits by means of controlled irrigation the same way that they may occur in dry-farmed vineyards. The positive effect of water deficit is mediated through abscisic acid (ABA) synthesis in the roots, which is best induced during long drying cycles. In irrigated vineyards, vine rooting is often shallow and the water supply to the vines is not buffered, meaning water becomes suddenly available immediately following an irrigation event, to become quickly reduced again, once the applied water is consumed. This drawback can be partly overcome when irrigation events are applied less frequently. Regulated deficit irrigation (RDI) and partial root zone drying (PRD) are also interesting irrigation strategies by which root ABA synthesis can be enhanced in irrigated vineyards (RDI: McCarthy, 1997; Dry et al., 2001; and PRD: Stoll et al., 2000).

Integrative indicators in terroir studies

Soil depth

Soil depth has a slightly different meaning for soil scientists and viticulturists. For soil scientists, soil depth represents the weathered layer above the parent rock. When vines are established, this layer is generally explored by the root system. For viticulturists, however, soil depth corresponds to rooting depth, which can extend beyond the weathered soil layer when parent material is either soft or contains cracks. The role of soil depth in terroir expression is often erroneously interpreted in many popular wine books, in which the terroir effect is attributed to deep rooting vines. The first vineyard soils to be studied on a scientific basis were from the Médoc area, Bordeaux (Seguin, 1969). In these sandy soils with high gravel content, the capacity of the soil to store water was so low that deep rooting was necessary to prevent vines from facing excessive water stress in dry summers. In a very popular wine atlas, Hugh Johnson (1979) published a soil profile from Seguin’s study but, unfortunately, from which many wine writers subsequently concluded that deep rooting is always a critical factor for terroir expression. In fact, in most situations, the relationship between rooting depth and wine quality is rather the opposite. When soils are not extremely poor, deep rooting provides access to unlimited water and possibly nitrogen, which increases vine vigor and yield. This then decreases the quality attributes of the grapes, in particular for red wine making, like anthocyanins and tannins. The effect of soil depth on grape quality was investigated by Morlat and Bodin (2006) and by Bodin and Morlat (2006) in the Loire Valley (France). These authors compared phenology, yield parameters and grape composition for three groups of vineyard soils with increasing depth: Weakly Weathered Rock (WWR), Moderately Weathered Rock (MWR) and Strongly Weathered Rock (SWR). The highest grape quality potential was obtained from WWR soils with limited depth and soil water availability. These conditions tended to make the soil temperature in the root zone higher, thereby enhancing precociousness of subsequent phenological stages and grape ripening curves. Similar results were obtained by Coipel et al. (2006) in the Rhône Valley, where highest quality potential for Grenache was obtained in shallow soils where nitrogen and water were more limited. For sites on hillsides, erosion is a key driver of soil depth (Brenot et al., 2008), shallow soils being located upslope and deeper colluvial soils distributed closer to and at the bottom. This is the case in Burgundy where the highest quality wines are produced at the middle and top parts of the slopes (Wilson, 1998). On the richer soils at the bottom of the slopes, lower quality wines are produced. Because vine performance is often closely related to soil depth it can be used as an integrative parameter in terroir studies. In some situations, soil depth can be mapped with electrical resistivity tomography (André et al., 2012).

It is not desirable, however, to have roots located in the top 20 cm of the soil, because this zone is generally too rich in nitrogen. Roots close to the soil surface may also pick up water from rainfall events close to the harvest date, with possible dilution of grape components. Managing the vineyard floor with the use of cover crops or mechanical weed destruction (tillage) tends to prevent roots from colonizing the layer close to the soil surface. Weed control with herbicides, on the other hand, can promote shallow root growth (Soyer et al., 1984).

Vine vigor

Vine vigor is driven by plant material (in particular the rootstock) and soil fertility. When plant material is homogeneous over a given area, vigor can be used as an indicator of the effect of environmental factors on the vine. Vigor can be easily mapped by means of remote sensing and used as a zoning tool, as described by Hall et al. (2003) and Bramley et al. (2011).

Management of terroir

Human factors in terroir expression

Seguin (1988) defined terroir as a cultivated ecosystem in which the vine interacts with factors from the natural environment, principally soil and climate. Because this ecosystem is cultivated, man plays a major role in terroir expression. He or she can orientate terroir expression through the choice of plant material and management practices. In this way, it is possible to manage terroir in order to maximize terroir expression in each location (van Leeuwen et al., 2016).

Indicators of major terroir parameters

Major soil-related terroir parameters are water and nitrogen supply to the vines as well as soil temperature. Many indicators of vine water and nitrogen status have been developed over the past decades (see Cifre et al., 2005 and van Leeuwen et al., 2009 for a review on indicators of vine water status and van Leeuwen et al., 2000 for a review on indicators of vine nitrogen status). Among these indicators, δ13C measured in grape juice is a convenient tool for assessing vine water status (Gaudillère et al., 2002; van Leeuwen et al., 2009) and Yeast Available Nitrogen (YAN) for assessing vine nitrogen status at high throughput (van Leeuwen et al., 2016). By means of these tools, vine water status (Figure 5) and vine nitrogen status (Figure 6) can be mapped at high resolution. In the latter example (from Château La Tour Carnet, appellation Haut-Médoc), the soils are gravelly-sandy and are rich in organic matter in the northern block, explaining greater water deficit and higher vine nitrogen status compared to the southern part, where soils are more clayey and lower in organic matter. Soil temperature can be measured, but because it is variable both spatially and temporally it is not easy to compute a relevant indicator. Warm and cool soils can be identified by expertise, as warm soils tend to be coarse textured and high in coarse elements. Because the relevant factor for soil temperature is the temperature in the root zone, shallow rooting soils can also be considered as warm soils.

Figure 5. Vine water status assessed by δ13C measured on grape sugar at harvest in a Bordeaux winegrowing estate in 2015 (Château La Tour Carnet). Map was obtained by Inverse Distance Weighting (IDW) interpolation from results from 10 samples/ha. A and B refer to vineyard blocks where A is located north of B.

Figure 6. Vine nitrogen status assessed by grape juice Yeast Available Nitrogen measured at harvest in a Bordeaux winegrowing estate in 2015 (Château La Tour Carnet, Haut-Médoc). Map was obtained by Inverse Distance Weighting (IDW) interpolation from results from 10 samples/ha. A and B refer to vineyard blocks where A north of B.

Management of vine water status

The production of high-quality red wines requires moderate water deficits. Frequently red wine grapes are negatively affected because of insufficient water deficits. There are no clear vine symptoms for this, so it can easily be overlooked by growers. In situations of excess vine water, the selection of soils with low SWHC and the implementation of training systems that increase transpiration (e.g. high planting density, high leaf area per hectare) may help to reach water deficit levels that promote wine quality. White varieties generally perform better in soils with high SWHC than red varieties (van Leeuwen, 2001). Installation of drainage tiles is only a partial solution, because they only allow evacuating water stored in macropores. In soils with high SWHC, large amounts of water are stored in micropores and drainage tiles have little effect. In dry climates, where excessive water stress may negatively impact yields and jeopardize wine quality, vineyard soils should have at least a medium SWHC. The choice of plant material is a powerful tool to adapt vineyards to drought, through the combination of drought-resistant rootstocks (Ollat et al., 2015) and drought-resistant cultivars (Schultz, 2003). Another possible adaptation to dry conditions is the use of the Mediterranean bush vine training system (also called the “gobelet”; Santesteban et al., 2017). When such adaptations still do not result in high-quality wines with economically sustainable yields, irrigation can be considered if there are adequate water resources available. Only deficit irrigation (when water supply does not meet climatic water demand), however, is compatible with terroir expression.

Management of vine nitrogen status

Vine nitrogen status is a terroir parameter easy to manage. When vine nitrogen status is very low, yield and vine vigor may be overly impacted. Red wine quality potential is rarely negatively impacted by low nitrogen availability, but important white wine aromas can be jeopardized. When vine nitrogen status is too low, it can be adjusted by organic or mineral fertilizers. If the vine nitrogen status is too high, it may provoke excessive vigor, thereby negatively impacting red wine quality potential and increasing susceptibility to grey rot (Botrytis cinerea). Cover crops can be an easy-to-implement solution to decrease vine vigor by acting as competitors for available nitrogen (Wheeler et al., 2005).

Management of soil temperature

Optimal terroir expression is closely related to the timing of ripeness of the grapes at the end of the season, avoiding high temperatures if too early and cool temperatures if too late (van Leeuwen and Seguin, 2006). The timing of ripeness is mainly driven by air temperature, but is also impacted by soil temperature, slope and aspect. When, in a given region, grapes tend to ripen too early, ripeness can be delayed by using later ripening varieties and long vegetative cycle rootstocks or by planting on north-facing slopes (south-facing slopes in the Southern Hemisphere). When grapes tend to ripen too late, the use of early ripening varieties and short cycle rootstocks may help to achieve full grape ripeness more regularly. When an important variety for a given region reaches ripeness at the end of the ripening window, planting in warm soils or on south-facing slopes (north-facing slopes in the Southern Hemisphere) should be preferred to reach full ripeness more easily.


The relationship between the sensory attributes of a wine and its origin is referred to as the “terroir” effect. Soil is a major factor in terroir expression, with its effect being mediated through the vine. Hence, soil-vine interactions have to be taken into account when studying the effect of soil on terroir expression. The soil effect has to be broken down into quantifiable components so as to measure its impact on grape composition and wine quality. Soil mainly influences grapevine phenology, vegetative and reproductive development, and grape composition through its effect on temperature in the root zone, as well as through its impact on vine water and nitrogen status. Over the past decades, tools have been developed to quantify these effects, both temporally and spatially. Once the major terroir parameters are quantified, growers can adapt their plant material and management practices accordingly so as to optimize terroir expression in their particular vineyard site.


Figures 5 and 6 were obtained in cooperation with SOVIVINS (Martillac, France). We are grateful to the staff of the Vignobles Bernard Magrez and its research and development unit for help with data acquisition for YAN, δ13C and vigor maps (Figures 2, 5 and 6). Analyses from Pauillac soil (Table 1a) were reproduced with kind permission from Olivier Trégoat and analyses from Mazis-Chambertin soil (Table 1b) with kind permission from ADAMA (Flavignerot, France).


  • André F., Van Leeuwen C., Saussez S., Van Durmen R., Bogaert P., Moghadas D., De Rességuier L., Delvaux B., Vereecken H. and Lambot S., 2012. High-resolution imaging of a vineyard in south of France, using ground penetrating radar, electromagnetic induction and electrical resistivity tomography. J. Appl. Geophys., 78, 113-122. doi:10.1016/j. jappgeo.2011.08.002
  • Baize D. and Girard M., 1995. Référentiel pédologique. INRA éditions, France.
  • Bodin F. and Morlat R., 2006. Characterization of viticultural terroirs using a simple field model based on soil depth. I – Validation of the water supply regime, phenology and vine vigour, in the Anjou vineyard (France). Plant Soil, 281, 37-54. doi:10.1007/ s11104-005-3768-0
  • Bokulich N.A., Thorngate J.H., Richardson P.M. and Mills D.A., 2014. Microbial biogeography of wine grapes is conditioned by cultivar, vintage, and climate. Proc. Natl. Acad. Sci. USA, 111, E139-E148. doi:10.1073/ pnas.1317377110
  • Bourguignon C., 1995. Le sol, la terre et les champs. Ed. Sang de la Terre.
  • Bramley R.G.V., Ouzman J. and Boss P.K., 2011. Variation in vine vigour, grape yield and vineyard soils and topography as indicators of variation in the chemical composition of grapes, wine and wine sensory attributes. Aust. J. Grape Wine Res., 17, 217-229. doi:10.1111/ j.1755-0238.2011.00136.x
  • Brenot J., Quiquerez A., Petit C. and Garcia J.-P., 2008. Erosion rates and sediment budgets in vineyards at 1-m resolution based on stock unearthing (Burgundy, France). Geomorphology, 100, 345-355. doi:10.1016/ j.geomorph. 2008.01.005
  • Choné X., van Leeuwen C., Chery P. and Ribéreau-Gayon P., 2001. Terroir influence on water status and nitrogen status of non-irrigated Cabernet-Sauvignon (Vitis vinifera): vegetative development, must and wine composition. S. Afr. J. Enol. Vitic., 22, 8-15.
  • Choné X., Lavigne-Cruège V., Tominaga T., van Leeuwen C., Castagnède C., Saucier C. and Dubourdieu D., 2006. Effect of vine nitrogen status on grape aromatic potential: flavor precursors (S-cysteine conjugates), glutathione and phenolic content in Vitis vinifera L. cv. Sauvignon blanc grape juice. J. Int. Sci. Vigne Vin, 40, 1-6. doi:10.20870/oeno-one.2006.40.1.880
  • Cifre J., Bota J., Escalona J.M., Medrano H. and Flexas J., 2005. Physiological tools for irrigation scheduling in grapevine (Vitis vinifera L.). An open gate to improve water-use efficiency? Agric. Ecosyst. Environ., 106, 159-170. doi:10.1016/j.agee.2004.10.005
  • Coipel J., Rodriguez-Lovelle B., Sipp C. and van Leeuwen C., 2006. Terroir effect, as a result of environmental stress, depends more on soil depth than on soil type (Vitis vinifera L. cv. Grenache noir, Côtes du Rhône, France, 2000). J. Int. Sci. Vigne Vin, 40, 177-185. doi:10.20870/oeno-one.2006.40.4.867
  • De Andres-De-Prado R., Yuste-Rojas M., Sort X., Andres-Lacueva C., Torres M. and Lamuela-Raventos R.M., 2007. Effect of soil type on wines produced from Vitis vinifera L. cv Grenache in commercial vineyards. J. Agric. Food Chem., 55, 779-786. doi:10.1021/jf062446q
  • Dry P.R., Loveys B.R., McCarthy M.G. and Stoll M., 2001. Strategic irrigation management in Australian vineyards. J. Int. Sci. Vigne Vin, 35, 129-139. doi:10.20870/oeno-one.2001.35.3.1699
  • Duchaufour P., 2001. Introduction à la science du sol. Ed. Dunod, Paris.
  • Dundon C.G., Smart R.E. and Mccarthy M.G., 1984. The effect of potassium fertilizer on must and wine potassium levels of Shiraz grapevines. Am. J. Enol. Vitic., 35, 200-205.
  • Duteau J., 1987. Contribution des réserves hydriques profondes du calcaire à Astéries compact à l’alimentation en eau de la vigne dans le Bordelais. Agronomie, 7, 859-865. doi:10.1051/agro:19871013
  • Duteau J., Guilloux M. and Seguin G., 1981. Influence des facteurs naturels sur la maturation du raisin, en 1979, à Pomerol et Saint-Émilion. Conn. Vigne Vin, 15, 1-27. doi:10.20870/oeno-one.1981.15.1.1358
  • Fanet J., 2001. Les terroirs du vin. Ed. Hachette, Paris.
  • Gaudillère J.-P., van Leeuwen C. and Ollat N., 2002. Carbon isotope composition of sugars in grapevine, an integrated indicator of vineyard water status. J. Exp. Bot., 53, 757-763. doi:10.1093/jexbot/53. 369.757
  • Gilbert J.A., van der Lelie D. and Zarraonaindia I., 2014. Microbial terroir for wine grapes. Proc. Natl. Acad. Sci. USA, 111, 5-6. doi:10.1073/pnas.1320471110
  • Hall A., Louis J. and Lamb D., 2003. Characterising and mapping vineyard canopy using high-spatial-resolution aerial multispectral images. Comput. Geosci., 29, 813-822. doi:10.1016/S0098-3004(03)00082-7
  • Helwi P., Habran A., Guillaumie S., Thibon C., Hilbert G., Gomès E., Delrot S., Darriet P. and van Leeuwen C., 2015. Vine nitrogen status does not have a direct impact on 2-methoxy-3-isobutylpyrazine in grape berries and wines. J. Agric. Food Chem., 63, 9789-9802. doi:10.1021/acs.jafc.5b03838
  • Helwi P., Guillaumie S., Thibon S., Keime C., Habran A., Hilbert G., Gomes E., Darriet P., Delrot S. and van Leeuwen C., 2016. Vine nitrogen status and volatile thiols and their precursors from plot to transcriptome level. BMC Plant Biol., 16, 173. doi:10.1186/s12870-016-0836-y
  • Huggett J., 2006. Geology and wine: a review. Proc. Geol. Assoc., 117, 239-247. doi:10.1016/S0016-7878 (06)80012-X
  • Johnson H., 1979. The world atlas of wine: a complete guide to the wines & spirits of the world. Ed. Mitchell Beazley, London.
  • Keller M., 2010. The science of grapevines: anatomy and physiology. Academic press.
  • Koundouras S., Marinos V., Gkoulioti A., Kotseridis Y. and van Leeuwen C., 2006. Influence of vineyard location and vine water status on fruit maturation of nonirrigated cv Agiorgitiko (Vitis vinifera L.). Effects on wine phenolic and aroma components. J. Agric. Food Chem., 54, 5077-5086. doi:10.1021/ jf0605446
  • Lebon E., Dumas V., Pieri P. and Schultz H.R., 2003. Modelling the seasonal dynamics of the soil water balance of vineyards. Funct. Plant Biol., 30, 699-710. doi:10.1071/FP02222
  • Maltman A., 2013. Minerality in wine: a geological perspective. J. Wine Res., 24, 169-181. doi:10.1080/ 09571264.2013.793176
  • Mccarthy M.G., 1997. The effect of transient water deficit on berry development of cv. Shiraz (Vitis vinifera L.). Aust. J. Grape Wine Res., 3, 2-8. doi:10.1111/j.1755-0238.1997.tb00128.x
  • Moran W., 2001. Terroir – the human factor. Aust. NZ Wine Ind. J., 16, 32-51.
  • Morlat R. and Bodin F., 2006. Characterization of viticultural terroirs using a simple field model based on soil depth. II – Validation of the grape yield and berry quality in the Anjou vineyard (France). Plant Soil, 281, 55-69. doi:10.1007/s11104-005-3769-z
  • Morris J.R., Sims C.A. and Cawthon D.L., 1983. Effects of excessive potassium levels on pH, acidity and color of fresh and stored grape juice. Am. J. Enol. Vitic., 34, 35-39.
  • Mundy D.C., 2008. A review of the direct and indirect effects of nitrogen on botrytis bunch rot in wine grapes. NZ Plant Protect., 61, 306-310. 61/nzpp_613060.pdf
  • OIV, 2010. Definition of terroir. public/medias/400/viti-2012-1-en.pdf. Accessed September 6, 2017.
  • Ojeda H., Deloire A. and Carbonneau A., 2001. Influence of water deficits on grape berry growth. Vitis, 40, 141-145. e046022.pdf
  • Ojeda H., Andary C., Kraeva E., Carbonneau A. and Deloire A., 2002. Influence of pre- and postveraison water deficit on synthesis and concentration of skin phenolic compounds during berry growth of Vitis vinifera cv. Shiraz. Am. J. Enol. Vitic., 53, 261-267.
  • Ollat N., Peccoux A., Papura D., Esmenjaud D., Marguerit E., Tandonnet J.-P., Bordenave L., Cookson S., Barrieu F., Rossdeutsch L., Lecourt J., Lauvergeat V., Vivin P., Bert P.-F. and Delrot S., 2015. Rootstocks as a component of adaptation to environment, pp. 68-108. In: Grapevine in a changing environment: a molecular and ecophysiological perspective. Geros H., Chaves M., Medrano H. and Delrot S. (Eds.), Wiley-Blackwell. doi:10.1002/97811187 35985.ch4
  • Ollé D., Guiraud J.L., Souquet J.M., Terrier N., Ageorges A., Cheynier V. and Verries C., 2011. Effect of pre- and post-veraison water deficit on proanthocyanidin and anthocyanin accumulation during Shiraz berry development. Aust. J. Grape Wine Res., 17, 90-100. doi:10.1111/j.1755-0238.2010.00121.x
  • Parker A., Garcia de Cortazar Atauri I., van Leeuwen C. and Chuine I., 2011. General phenological model to characterise the timing of flowering and veraison of Vitis vinifera L. Aust. J. Grape Wine Res., 17, 206-216. doi:10.1111/j.1755-0238.2011.00140.x
  • Parker A., Garcia de Cortázar-Atauri I., Chuine I., Barbeau G., Bois B., Boursiquot J.-M., Cahurel J. Y., Claverie M., Dufourcq T., Gény L., Guimberteau G., Hofmann R., Jacquet O., Lacombe T., Monamy C., Ojeda H., Panigai L., Payan J.-C., Rodriquez-Lovelle B., Rouchaud E., Schneider C., Spring J.-L., Storchi P., Tomasi D., Trambouze W., Trought M. and van Leeuwen C., 2013. Classification of varieties for their timing of flowering and veraison using a modelling approach. A case study for the grapevine species Vitis vinifera L. Agric. For. Meteorol., 180, 249-264. doi:10.1016/j.agrformet.2013.06.005
  • Pellegrino A., Lebon E., Simonneau T. and Wery J., 2005. Towards a simple indicator of water stress in grapevine (Vitis vinifera L.) based on the differential sensitivities of vegetative growth components. Aust. J. Grape Wine Res., 11, 306-315. doi:10.1111/j.1755-0238.2005.tb00030.x
  • Peyrot des Gachons C., van Leeuwen C., Tominaga T., Soyer J.-P., Gaudillère J.-P. and Dubourdieu D., 2005. Influence of water and nitrogen deficit on fruit ripening and aroma potential of Vitis vinifera L. cv Sauvignon blanc in field conditions. J. Sci. Food Agric., 85, 73-85. doi:10.1002/jsfa.1919
  • Picard M., van Leeuwen C., Guyon F., Gaillard L., De Revel G. and Marchand S., 2017. Vine water deficit impacts aging bouquet in fine red Bordeaux wine. Front. Chem., 5, 56. doi:10.3389/fchem.2017.00056
  • Pons A., Allamy L., Schüttler A., Rauhut D., Thibon C. and Darriet P., 2017. What is the expected impact of climate change on wine aroma compounds and their precursors in grape? OENO One, 51, 141-146. doi:10.20870/oeno-one.2017.51.2.1868
  • Renouf V., Trégoat O., Roby J.-P. and van Leeuwen C., 2010. Soils, rootstocks and grapevine varieties in prestigious Bordeaux vineyards and their impact on yield and quality. J. Int. Sci. Vigne Vin, 44, 127-134. doi:10.20870/oeno-one.2010.44.3.1471
  • Santesteban L.G., Miranda C., Urrestarazu J., Loidi M. and Royo J., 2017. Severe trimming and enhanced competition of laterals as a tool to delay ripening in Tempranillo vineyards under semiarid conditions. OENO One, 51, 191-203. doi:10.20870/oeno-one.2017.51.2.1583
  • Saxton K., Rawls W., Romberger J. and Papendick R., 1986. Estimating generalized soil-water characteristics from texture. Soil Sci. Soc. Am. J., 50, 1031-1036. doi:10.2136/sssaj1986.0361599500 5000040039x
  • Schultz H., 2003. Differences in hydraulic architecture account for near-isohydric and anisohydric behaviour of two field-grown Vitis vinifera L. cultivars during drought. Plant Cell Environ., 26, 1393-1405. doi:10.1046/j.1365-3040.2003. 01064.x
  • Seguin G., 1969. L’alimentation en eau de la vigne dans des sols du Haut-Médoc. Conn. Vigne Vin, 3, 93-141. doi:10.20870/oeno-one.1969.3.2.1949
  • Seguin G., 1986. “Terroirs” and pedology of wine growing. Experientia, 42, 861-873. doi:10.1007/ BF01941763
  • Seguin G., 1988. Ecosystems of the great red wines produced in the maritime climate of Bordeaux, pp. 36-53. In: Proceedings of the Symposium on Maritime Climate Winegrowing. Fuller-Perrine L. (Ed.). Department of Horticultural Sciences, Cornell University, Geneva, NY.
  • Soyer J.-P. and Molot C., 1993. Fertilisation potassique et composition des moûts ; évolution durant la maturation du raisin. Prog. Agric. Vitic., 110, 174-177.
  • Soyer J.-P., Delas J., Molot C., Andral P. and Casteran P., 1984. Techniques d’entretien du sol en vignoble Bordelais. Prog. Agric. Vitic., 101, 315-320.
  • Spayd S., Wample R., Stevens R., Evans R. and Kawakami A., 1993. Nitrogen fertilization of white Riesling in Washington. Effects on petiole nutrient concentration, yield, yield components, and vegetative growth. Am. J. Enol. Vitic., 44, 378-386.
  • Spayd S., Wample R., Evans R., Stevens R., Seymour B. and Nagel C., 1994. Nitrogen fertilization of white Riesling grapes in Washington. Must and wine composition. Am. J. Enol. Vitic., 45, 34-41.
  • Steenwerth K. and Belina K., 2008. Cover crops enhance soil organic matter, carbon dynamics and microbiological function in a vineyard agroeco-system. Appl. Soil Ecol., 40, 359-369. doi:10.1016/ j.apsoil.2008.06.006
  • Stoll M., Loveys B. and Dry P., 2000. Hormonal changes induced by partial rootzone drying of irrigated grapevine. J. Exp. Bot., 51, 1627-1634. doi:10.1093/ jexbot/51.350.1627
  • Storchi P., Costantini E. and Bucelli P., 2005. The influence of climate and soil on viticultural and enological parameters of Sangiovese grapevines under non-irrigated conditions. Acta Hortic., 689, 333-340. doi:10.17660/ActaHortic.2005.689.39
  • Tesic D., Woolley D.J., Hewett E.W. and Martin D.J., 2002. Environmental effects on cv. Cabernet-Sauvignon (Vitis vinifera L.) grown in Hawke’s Bay, New Zealand. 2. Development of a site index. Aust. J. Grape Wine Res., 8, 27-35. doi:10.1111/j.1755-0238.2002.tb00208.x
  • Tramontini S., van Leeuwen C., Domec J.-C., Destrac-Irvine A., Basteau C., Vitali M., Mosbach-Schulz O. and Lovisolo C., 2013. Impact of soil texture and water availability on the hydraulic control of plant and grape-berry development. Plant Soil, 368, 215-230. doi:10.1007/s11104-012-1507-x
  • Trégoat O., 2003. Caractérisation du régime hydrique et du statut azoté de la vigne par des indicateurs physiologiques dans une étude de terroir au sein de huit grands crus de Bordeaux. Influence sur le comportement de la vigne et la maturation du raisin. Diplôme d’Etudes et de Recherches de l’Université Bordeaux 2.
  • Trégoat O., van Leeuwen C., Choné X. and Gaudillère
  • J.-P., 2002. Étude du régime hydrique et de la nutrition azotée de la vigne par des indicateurs physiologiques. Influence sur le comportement de la vigne et la maturation du raisin (Vitis vinifera L. cv Merlot, 2000, Bordeaux). J. Int. Sci. Vigne Vin, 36, 133-142. doi:10.20870/oeno-one.2002.36.3.967
  • van Leeuwen C., 2001. Choix du cépage en fonction du terroir dans le Bordelais. J. Int. Sci. Vigne Vin, Hors Série (Un raisin de qualité : de la vigne à la cuve), 97-102.
  • van Leeuwen C., 2010. Terroir: the effect of the physical environment on vine growth, grape ripening and wine sensory attributes, pp. 273-315. In: Managing wine quality, volume 1: Viticulture and wine quality. Reynolds A. (Ed.), Woodhead Publishing Ltd., Oxford, UK. doi:10.1533/9781845699284.3.273
  • van Leeuwen C. and Seguin G., 1994. Incidences de l’alimentation en eau de la vigne, appréciée par l’état hydrique du feuillage, sur le développement de l’ppareil végétatif et la maturation du raisin (Vitis vinifera variété Cabernet franc, Saint-Émilion, 1990). J. Int. Sci. Vigne Vin, 28, 81-110. doi:10.20870/oeno-one.1994.28.2.1152
  • van Leeuwen C. and Seguin G., 2006. The concept of terroir in viticulture. J. Wine Res., 17, 1-10. doi:10.1080/09571260600633135
  • van Leeuwen C., Baudet D., Duteau J., Seguin G. and Wilbert J., 1989. Les sols viticoles et leur répartition à Saint-Emilion, Pomerol et quelques autres communes du Libournais. J. Int. Sci. Vigne Vin, 23, 131-150. doi:10.20870/oeno-one.1989.23.3.1243
  • van Leeuwen C., Friant Ph., Soyer J.-P., Molot C., Choné X. and Dubourdieu D., 2000. L’intérêt du dosage de l’azote total et l’azote assimilable dans le moût comme indicateur de la nutrition azotée de la vigne. J. Int. Sci. Vigne Vin, 34, 75-82. doi:10.20870/ oeno-one.2000.34.2.1010
  • van Leeuwen C., Friant Ph., Chone X., Trégoat O., Koundouras S. and Dubourdieu D., 2004. Influence of climate, soil and cultivar on terroir. Am. J. Enol. Vitic., 55, 207-217.
  • van Leeuwen C., Trégoat O., Choné X., Bois B., Pernet D. and Gaudillère J.-P., 2009. Vine water status is a key factor in grape ripening and vintage quality for red Bordeaux wine. How can it be assessed for vineyard management purposes? J. Int. Sci. Vigne Vin, 43, 121-134. doi:10.20870/oeno-one.2009. 43.3.798
  • van Leeuwen C., Roby J.P., Pernet D. and Bois B., 2010. Methodology of soil-based zoning for viticultural terroirs. Bull. O.I.V., 83, 13-29.
  • van Leeuwen C., Roby J.-Ph. and De Resseguier L., 2016. Understanding and managing wine production from differents terroirs. XIth International Terroir Congress, Willamette Valley, 10-14 July 2016, Oregon, USA.
  • Wheeler S., Black A. and Pickering G., 2005. Vineyard floor management improves wine quality in highly vigorous Vitis vinifera ‘Cabernet-Sauvignon’ in New Zealand. NZ J. Crop Hortic. Sci., 33, 317-328. doi:10.1007/s11104-012-1507-x
  • White R., 2003. Soils for fine wines. Oxford University Press, New York.
  • Wilson J., 1998. Terroir: the role of geology, climate and culture in the making of French wines. Ed. Mitchell Beazley, London.


Cornélis van Leeuwen

Country : France

Biography :

Kees (Cornelis van Leeuwen) is a professor of viticulture at Bordeaux Sciences Agro, which makes part of Bordeaux University’s Institut des Sciences de la Vigne et du Vin. Kees van Leeuwen conducts research on the concept of terroir in viticulture. His works are centred on environmental constraint in the expresssion of vine-growing terroir. This constraint is most often a limiting of water supply or a limiting of nitrogen nutrition in the vines. Kees van Leeuwen has taken part in the creation and evaluation of several indicators of water supply regime and nitrogen status in vines. Kees van Leeuwen has also worked on the climate’s effect on the expression of vine-growing terroir. The vine’s response is evaluated through the precocity of its vegetation, its growth and development and its grapes constituents at ripeness. Particular attention is paid to the grapes’ aromatic potential in relation to environmental factors. He participated in the creation of the Grapevine Flowering Veraison model (GFV model).
Kees van Leeuwen is a consultant for Château Cheval Blanc in Saint-Émilion. He has carried out or taken part in numerous studies to map the different soils of wine estates and appellations. Kees van Leeuwen was the editor-in-chief of the Journal International des Sciences de la Vigne et du Vin from 2001 to 2016. He writes on a regular basis for the Dutch magazine « Perswijn ».

Jean-Philippe Roby

Affiliation : EGFV, Bordeaux Sciences Agro, INRA, Univ. Bordeaux, ISVV, 33883 Villenave d’Ornon, France

Country : France

Laure de Rességuier

Affiliation : EGFV, Bordeaux Sciences Agro, INRA, Univ. Bordeaux, ISVV, 33883 Villenave d’Ornon, France

Country : France


No supporting information for this article

Article statistics

Views: 11840


PDF: 2132

XML: 117